
CNR4 Net Radiometer
colder. This means that for estimating the far infrared radiation that is
generated by the object that is faced by the pyrgeometer, usually the sky or the
soil, you will have to take the pyrgeometer temperature, T, into account. This
is why the temperature sensors are incorporated in the CNR4's body near the
pyrgeometer sensing element, and has, therefore, the same temperature as the
pyrgeometer sensor surface. The calculation of the long-wave far infrared
irradiance, E, is done according to the following equation:
For the pyrgeometer only
E = V/C + 5.67·10-8·T4 (5-2)
In this equation C is the sensitivity of the sensor. Please bear in mind that T is
in Kelvin, and not in Celsius or Fahrenheit.
The downward-facing pyrgeometer measures the far infrared radiation that is
emitted by the ground. The upward-facing pyrgeometer measures the far
infrared radiation from the sky. As the sky is typically colder than the
instrument, one can expect negative voltage signals from the upward-facing
pyrgeometer. The Equation 5-2 is used to calculate the far infrared irradiance
of the sky and of the ground.
5.3 Measuring CNR4 Temperature with Thermistor
The CNR4 has two temperature sensors built inside: thermistor and Pt-100.
They both have the identical accuracy. We recommend using the thermistor
with Campbell Scientific dataloggers. The thermistor has a larger resistance
(10 kΩ@ 25°C) than Pt-100 sensor (100 Ω@ 0°C), and the change in
resistance with respect to temperature, in absolute terms, is greater. Therefore,
the cable resistance can be neglected, and the thermistor can easily be
measured using half-bridge measurement instruction on Campbell Scientific
dataloggers. This makes it simpler to program, and uses fewer measurement
channels.
Table 5-1 shows the thermistor resistance values as a function of temperature.
Relatively small errors occur when the CNR4 is not in thermal equilibrium.
This happens for example when the heater is on, or when the sun is shining.
When the heater and ventilator are on, the largest expected deviation between
the real sensor temperature and the thermistor reading is 1 degree. This results
in a worst case error for the pyrgeometer of 5 W/m2. When the sun is shining,
the largest expected deviation between the real sensor temperature and the
thermistor reading is again 1 degree. This results in a worst case error for the
pyrgeometer of 5 W/m2.
The thermistor will not give a good indication of ambient air temperature; at
1000 W/m2solar radiation, and no wind, the instrument temperature will rise
approximately 5 degrees above the ambient temperature.
The offsets of both the pyranometers and the pyrgeometers might be larger
than 5W/m2if large temperature gradients are forced on the instrument (larger
than 5 K/hr). This happens for example when rain hits the instrument. The
occurrence of this can be detected using the thermistor readout, and can be
used for data filtering.
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